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Priscomyzon Temporal range: Famennian | |
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Genus: | Priscomyzon Gess et al., 2006 |
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Priscomyzon riniensis Gess et al., 2006 |
Priscomyzon riniensis is an extinct lamprey that lived some 360 million years ago during the Famennian (Late Devonian) in a marine or estuarine environment in South Africa. This small agnathan is anatomically similar to the Mazon Creek lampreys, but is some 35 million years older. Its key developments included the first known large oral disc, circumoral teeth and a branchial basket.
Though common and diverse during the Silurian and Devonian, jawless fish are today represented only by lampreys and hagfish, both groups being quite specialized. Lampreys have seven gill pouches (whereas jawed fish have only five), no paired fins, and a rudimentary skeleton of cartilage. They also have a sucker disc of cartilage surrounded by a soft lip and a central small mouth set about with simple hooked teeth. They attach to the bodies of other vertebrates by suction, securing their grip with the hooked teeth, after which a rasped tongue scrapes a hole providing access to the host's softer tissues.
Priscomyzon provides evidence that agnathans close to modern lampreys had existed before the end of the Devonian period. Lampreys have ancient origins, have endured for 360 million years and lived through four major extinction events - even so, their evolutionary history is obscure. In ancient seas jawless vertebrate fish led to jawed fish, and thence to all other vertebrates, including humans. Being the only extant jawless vertebrates and a virtual time capsule of embryology and DNA, lampreys and hagfish are of immense scientific interest. [1] Knowing the period during which they became parasitic would shed light on how typical they are of ancient fish. Having no bone tissue, effectively being essentially boneless, their cartilaginous framework leaves almost no fossil record - a mere three fossil species had previously been described, and in none of these was a sucker disc detected.
The exceptionally well-preserved fossil of P. riniensis is only 42 millimetres (1.7 in) long and reveals details of its fin, gill basket and mouth region. A striking feature of Priscomyzon is its relatively large oral disk, inside a soft outer lip, supported by annular cartilage. The circular mouth at the center of the oral disk is surrounded by 14 small, evenly spaced, simple teeth, with no associated radiating series or plates of supplementary teeth, but otherwise quite similar to present-day lampreys, suggesting that their blood-sucking lifestyle was developed in ancient seas. The oral disk of the Late Carboniferous lamprey Mayomyzon pieckoensis , if present, is much smaller, while there is no evidence of a disk in the Early Carboniferous Hardistiella montanensis . Priscomyzon's are the earliest teeth found in any fossil lamprey, and have a similar arrangement to that of the 19 or more teeth found in modern forms such as Ichthyomyzon , Petromyzon , Caspiomyzon and Geotria . [2]
Its posterior teeth are more elongate than the rest, while in modern species lateral or anterior teeth tend to be largest. Its teeth are also quite simple in shape compared to those of modern species, and in this respect are probably primitive. The position of the orbits is not clear as there are no darkened areas suggesting eye locations. The branchial imprint is preserved in great detail, parts of both the right and left baskets having been preserved, and the posterior five branchial arches being well defined. Anterior to these the presence of seven branchial pouches is evident. The dorsal fin originates immediately behind the branchiae and continues to the caudal extremity, resembling a modern ammocoete or lamprey larva rather than an adult, in which separate anterior and posterior dorsal fins are to be found. [2]
Fossils of juvenile specimens indicate that it did not have the filter feeding "ammocoete" juvenile stage found in modern lampreys, with juveniles morphologically similar to adults. [3]
The lamprey fossil was discovered on Waterloo Farm in rocks of the Witteberg Group near Grahamstown in South Africa. The species was described by Robert W. Gess & Bruce S. Rubidge of the Bernard Price Institute (Palaeontology) Wits University, and Michael I. Coates of the Department of Organismal Biology University of Chicago in the journal Nature of 26 October 2006. The shale containing the fossil was discovered as far back as 1985 during construction of the N2 bypass outside Grahamstown. The site consists of black carbonaceous shale formed from anaerobic mud deposited in a marine estuary on the Agulhas Sea. A variety of organic remains are found in this setting, including algae, terrestrial plants and fish. Invertebrate remains are of small bivalves, ostracods, clam shrimp, and a eurypterid. Fossil material has been greatly compressed and original tissue replaced by metamorphic mica altered to chlorite during uplift. To prevent rockfalls onto the road from the unstable formation, the steep slopes were cut back again in 1999 and once more in 2007/8. During these upgrades Gess managed to obtain a large sample of rock blocks with the help of the road construction company, and worked intermittently on exposing their contents.
The scientific name derives from the Latin priscus "ancient", and Greek myzon "sucking". 'Rini' is the isiXhosa name for Grahamstown and its surrounding valley.
The holotype is held in the Albany Museum, Grahamstown, Eastern Cape, with the catalogue number AM5750. The locality and horizon is the Waterloo Farm, Grahamstown, South Africa; Witpoort Formation, Witteberg Group, Famennian, Late Devonian.
Hagfish, of the class Myxini and order Myxiniformes, are eel-shaped jawless fish. Hagfish are the only known living animals that have a skull but no vertebral column, although they do have rudimentary vertebrae. Hagfish are marine predators and scavengers who can defend themselves against other larger predators by releasing copious amounts of slime from mucous glands in their skin.
Agnatha is a paraphyletic infraphylum of non-gnathostome vertebrates, or jawless fish, in the phylum Chordata, subphylum Vertebrata, consisting of both living (cyclostomes) and extinct. Among recent animals, cyclostomes are sister to all vertebrates with jaws, known as gnathostomes.
Gnathostomata are the jawed vertebrates. Gnathostome diversity comprises roughly 60,000 species, which accounts for 99% of all living vertebrates, including humans. Most gnathostomes have retained ancestral traits like true teeth, a stomach, and paired appendages. Other traits are elastin, a horizontal semicircular canal of the inner ear, myelin sheaths of neurons, and an adaptive immune system which has discrete lymphoid organs, and uses V(D)J recombination to create antigen recognition sites, rather than using genetic recombination in the variable lymphocyte receptor gene.
Cephalaspidomorphs are a group of jawless fishes named for Cephalaspis of the osteostracans. Most biologists regard this taxon as extinct, but the name is sometimes used in the classification of lampreys, because lampreys were once thought to be related to cephalaspids. If lampreys are included, they would extend the known range of the group from the Silurian and Devonian periods to the present day. They are the closest relatives of jawed fishes, who may have emerged from within them; if this is true, they would survive if the jawed fish are included.
Thelodonti is a class of extinct Palaeozoic jawless fishes with distinctive scales instead of large plates of armor.
The class Osteostraci is an extinct taxon of bony-armored jawless fish, termed "ostracoderms", that lived in what is now North America, Europe and Russia from the Middle Silurian to Late Devonian.
Cyclostomi, often referred to as Cyclostomata, is a group of vertebrates that comprises the living jawless fishes: the lampreys and hagfishes. Both groups have jawless mouths with horny epidermal structures that function as teeth called ceratodontes, and branchial arches that are internally positioned instead of external as in the related jawed fishes. The name Cyclostomi means "round mouths". It was named by Joan Crockford-Beattie.
Groenlandaspis is an extinct genus of arthrodire from the Late Devonian. Fossils of the different species are found in late Devonian strata in all continents except eastern Asia. The generic name commemorates the fact that the first specimens of the type species were found in Greenland.
Marine vertebrates are vertebrates that live in marine environments. These are the marine fish and the marine tetrapods. Vertebrates are a subphylum of chordates that have a vertebral column (backbone). The vertebral column provides the central support structure for an internal skeleton. The internal skeleton gives shape, support, and protection to the body and can provide a means of anchoring fins or limbs to the body. The vertebral column also serves to house and protect the spinal cord that lies within the column.
Lampreys are a group of jawless fish comprising the order Petromyzontiformes. The adult lamprey is characterized by a toothed, funnel-like sucking mouth. The common name "lamprey" is probably derived from Latin lampetra, which may mean "stone licker", though the etymology is uncertain. Lamprey is sometimes seen for the plural form.
Most bony fishes have two sets of jaws made mainly of bone. The primary oral jaws open and close the mouth, and a second set of pharyngeal jaws are positioned at the back of the throat. The oral jaws are used to capture and manipulate prey by biting and crushing. The pharyngeal jaws, so-called because they are positioned within the pharynx, are used to further process the food and move it from the mouth to the stomach.
The evolution of fish began about 530 million years ago during the Cambrian explosion. It was during this time that the early chordates developed the skull and the vertebral column, leading to the first craniates and vertebrates. The first fish lineages belong to the Agnatha, or jawless fish. Early examples include Haikouichthys. During the late Cambrian, eel-like jawless fish called the conodonts, and small mostly armoured fish known as ostracoderms, first appeared. Most jawless fish are now extinct; but the extant lampreys may approximate ancient pre-jawed fish. Lampreys belong to the Cyclostomata, which includes the extant hagfish, and this group may have split early on from other agnathans.
Gondwanascorpio emzantsiensis is an extinct Gondwanan scorpion that lived 360 million years ago in the Devonian. Its fossil remains, clearly showing pincer and sting, were discovered in rocks of the Witteberg Group near Grahamstown in South Africa. At present, this scorpion is the oldest known land-dwelling animal from Gondwana, which in Devonian times was separated from Laurasia by a deep ocean. At the time, the fossil site was only 15° from the South Pole, but rather than arctic-like tundra, the region was probably wooded, providing ample insect life for food. Previously, only two scorpion species were known from the late Devonian – Hubeiscorpio gracilitarsus from China and Petaloscorpio bureaui from Canada. The species was described by Robert Gess of Wits University in the journal African Invertebrates. The specific epithet derives from umZantsi, the isiXhosa word for "south", sometimes used for South Africa.
Serenichthys kowiensis is a fossil species of coelacanth described in 2015 from near Grahamstown in South Africa.
Antarctilamna is an extinct genus of Devonian cartilaginous fish originally exemplified by Antarctilamna prisca from South Eastern Australia and Antarctica. The latest occurring described species is Antarctilamna ultima from the Waterloo Farm lagerstätte in South Africa. Antarctilamna has robust ctenacanthid-like spines which lack a deep insertion area, and are borne in front of the first dorsal fin; in addition to distinctive diplodont teeth with small intermediate cusps. Antarctilamna-like spines, known from the Bunga Beds locality in Australia have been ascribed to A. prisca.
The Waterloo Farm lagerstätte is a Famennian lagerstätte in South Africa that constitutes the only known record of a near-polar Devonian coastal ecosystem.
Diplacanthus is an extinct genus of Mid to Late Devonian fish in the class Acanthodii, known as spiny sharks.
Hexachara is a genus of fossil charophyte that is likely to have formed meadows within sheltered oligohaline reaches of lakes.
Panderodus Is an extinct genus of jawless fish belonging to the order Conodonta. This genus had a long temporal range, surviving from the middle Ordovician to late Devonian. In 2021, extremely rare body fossils of Panderodus from the Waukesha Biota were described, and it revealed that Panderodus had a more thick body compared to the more slender bodies of more advanced conodonts. It also revealed that this conodont was a macrophagous predator, meaning it went after large prey.
Achanarella is a genus of extinct jawless fish from the Achanarras Quarry in Scotland, dating to the Middle Devonian. The only known species in the genus is Achanarella trewini.